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基于InSAR数据的北京地铁6号线地面沉降监测分析
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  • 英文篇名:Monitoring and Analysis of Land Subsidence of Beijing Metro Line 6 Based on InSAR Data
  • 作者:刘凯斯 ; 宫辉力 ; 陈蓓蓓
  • 英文作者:LIU Kaisi;GONG Huili;CHEN Beibei;Key Lab of 3D Information Acquisition and Application, Ministry of Education;The State Key Laboratory of Breeding Base of Process of Urban Environment and Digital Simulation;College of Resource Environment and Tourism, Capital Normal University;
  • 关键词:PS-InSAR ; 地面沉降 ; 层次熵值法
  • 英文关键词:PS-InSAR;;land subsidence monitoring;;hierarchical entropy method
  • 中文刊名:DQXX
  • 英文刊名:Journal of Geo-Information Science
  • 机构:三维信息获取与应用教育部重点实验室;城市环境过程数字模拟国家重点实验室培育基地;首都师范大学资源环境与旅游学院;
  • 出版日期:2018-02-01 13:49
  • 出版单位:地球信息科学学报
  • 年:2018
  • 期:v.20;No.125
  • 基金:国家自然科学基金重点项目(41130744);国家自然科学基金面上项目(41171335);国家自然科学基金项目(4140010982)~~
  • 语种:中文;
  • 页:DQXX201801015
  • 页数:10
  • CN:01
  • ISSN:11-5809/P
  • 分类号:132-141
摘要
本文以北京市地铁6号线为研究区,采用PS-In SAR技术对研究区53景Terra SAR影像进行永久散射体干涉处理,获取了研究区地面沉降信息,初步揭示了线状研究区的地面沉降空间分布特征,进一步结合层次熵值法,定位6号线典型路段,深入分析了地面沉降发展的严重程度及不均匀性。研究结果表明:(1)6号线沿线自西向东沉降速率增大,最大年沉降速率为77.2 mm/a,出现在常营—草房路段;(2)综合熵值以金台路站为分界,西侧熵值小(小于0.5),东侧接近或大于1,金台路以东路段沉降量大,且不均匀沉降严重;(3)在地质条件相似的金台路-十里堡、青年路-褡裢坡、黄渠-草房3个路段内,沉降严重程度同时受年沉降速率、斜率、曲率半径变化驱动,且相关性强。
        In this paper, we choose the Beijing Metro Line 6 as the study area. The land subsidence is obtained by using PS-In SAR technique, and the spatial distribution characteristics of subsidence in the study area are analyzed. We further combine hierarchical entropy method to locate the typical section of Line 6. The severity and uneven of subsidence is also analyzed. The main conclusions are as follows:(1) The rate of subsidence from west to east along the line 6 is gradually increasing, and annual maximum subsidence rate is 77.2 mm/a, which appears in the Chang Ying-Cao Fang section;(2) The integrated entropy is divided by the Jin Tai Lu Station, the west side has a small entropy(less than 0.5), and the east side is close to 1 or greater than 1. The subsidence of the east side of Jin Tai Lu Station is serious. It is pronounced uneven subsidence.(3) In the three sections of Jin Tai Lu-Shi Li Pu, Qing Nian Lu-Da Lian Po, Huang Qu-Cao Fang, the subsidence severity is affected by the annual subsidence rate, slope, curvature radius, and the correlation is strong.
引文
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